IMAGE  EVALUATION 
TEST  TARGET  (MT-3) 


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23  WEST  MAIN  STREET 

WEBSTER,  NY.  14580 

(716)  873-4503 


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CIHM/ICMH 

Microfiche 

Series. 


CIHM/ICMH 
Collection  de 
microfiches. 


Canadian  Institute  for  Historical  Microreproductions  /  Institut  Canadian  de  microreproductions  historiques 


i 


Technical  and  Bibliographic  Notes/Notes  techniques  et  bibliographiques 


The  Institute  has  attempted  to  obtain  the  best 
original  copy  available  for  filming.  Features  of  this 
copy  which  may  be  bibliographically  iinique, 
which  may  alter  any  of  the  images  in  the 
reproduction,  or  which  may  significantly  change 
the  usual  method  of  filming,  are  checked  below. 


D 
D 
D 
D 
D 
[3 

D 
D 
D 

D 


□ 


Coloured  covers/ 
Couverture  de  couleur 

Covers  damaged/ 
Couverture  endommag6e 

Covers  restored  and/or  laminated/ 
Couverture  restaurie  et/ou  pellicul6e 

Cover  title  missing/ 

Le  titre  de  couverture  manque 

Coloured  maps/ 

Cartes  q6ographiques  en  couleur 

Coloured  ink  (i.e.  other  than  blue  or  black)/ 
Encre  de  couleur  (i.e.  autre  qun  bleue  ou  noire) 

Coloured  plates  and/or  illustrations/ 
Planches  et/ou  illustrations  en  couleur 

Bound  with  other  material/ 
ReliA  avec  d'autres  documents 

Tight  binding  may  cause  shadows  or  distortion 
along  interior  margin/ 

La  reliure  serr^e  peut  causer  de  I'ombre  ou  de  la 
distortion  le  long  de  la  marge  int^rieure 

Blank  leaves  added  during  restoration  may 
appear  within  the  text.  Whenever  possible,  these 
have  been  omitted  from  filming/ 
II  se  peut  que  certaines  pages  blanches  ajouties 
lors  d'une  restauration  apparaissent  dans  la  texte. 
mals,  lorsque  cela  6tait  possible,  ces  pages  n'ont 
pas  iti  filmAes. 

Additional  comments:/ 
Commentaires  supplAmentaires; 


L'Institut  a  microfilm^  le  meilleur  exemplaire 
qu'il  lui  a  6t6  possible  de  se  procurer.  Les  details 
de  cat  exemplaire  qui  sont  peut-dtre  uniques  du 
point  de  vue  bibliographique,  qui  peuvent  modifier 
une  image  reprodi<ite,  ou  qui  peuvent  exiger  une 
modification  dans  la  m6thode  normale  de  filmage 
sont  indiqu6s  ci-dessous. 


T 
t( 


I      I   Coloured  pages/ 


Pages  de  couleur 

Pages  damaged/ 
Pages  endommagies 

Pages  restored  and/oi 

Pages  restauries  et/ou  peilicuides 

Pages  discoloured,  stained  or  foxet 
Pages  d^colories,  tachet^es  ou  piqu^es 

Pages  detached/ 
Pages  ddtachdes 

Showthrough/ 
Transparence 

Quality  of  prir 

Qualitd  indgale  de  I'impression 

Includes  supplementary  materit 
Comprend  du  materiel  suppl^mentaire 

Only  edition  available/ 
Seule  Edition  disponible 


I      I  Pages  damaged/ 

I      I  Pages  restored  and/or  laminated/ 

I      I  Pages  discoloured,  stained  or  foxed/ 

I      I  Pages  detached/ 

r  "1  Showthrough/ 

I      I  Quality  of  print  varies/ 

I      I  Includes  supplementary  material/ 

I — I  Only  edition  available/ 


Ti 
P 

O' 

fl 


O 

b( 
th 
si 
ot 
fii 
sii 
oi 


sh 
TI 

wl 

M 
dij 
en 
be 
rifl 
rei 
m« 


D 


Pages  wholly  or  partially  obscured  by  errata 
slips,  tissues,  etc.,  have  been  refilmed  to 
ensure  the  best  possible  image/ 
Les  pages  .'otulement  ou  partiellement 
obscurcies  ^lar  un  feuillet  d'errata,  une  pelure, 
etc..  ont  6tA  filmAes  A  nouveau  de  fa^on  A 
obtenir  la  m'iilleure  image  possible. 


This  item  is  filmed  at  the  reduction  ratio  checked  below/ 

Ce  document  est  film*  au  taux  de  reduction  indiquA  ci-defYOus. 

10X  14X  18X  22X 


C 


TT 


12X 


16X 


20X 


26X 


30X 


a4x 


28X 


n 

32X 


Tha  copy  filmad  hers  has  baan  raproducad  thanks 
to  tha  ganarosity  of: 

Library  Division 

Provincial  Archives  of  British  Columbia 

Tha  imagas  appaaring  hara  ara  tha  bast  quality 
possibia  considaring  tha  condition  and  lagibility 
of  tha  original  copy  and  In  kaaping  with  tha 
filnr>ing  contract  spacifications. 


Original  copias  in  printad  papar  covars  ara  filmad 
baginning  with  tha  front  covar  and  anding  on 
tha  last  paga  with  a  printad  or  illustratad  impras- 
sion,  or  tha  back  covar  whan  appropriata.  Ail 
othar  original  copias  ara  filmad  baginning  on  tha 
first  paga  with  a  printad  or  illustratad  impras- 
sion,  and  anding  on  tha  last  paga  with  a  printad 
or  illustratad  imprassion. 


Tha  last  racordad  frame  on  each  microfiche 
shall  contain  the  symbol  -^  (meaning  "CON- 
TINUED"), or  the  symbol  V  (meaning  "END"), 
whichever  applies. 

Maps,  plates,  charts,  etc.,  may  be  filmed  at 
different  reduction  ratios.  Those  too  large  to  be 
entirely  included  in  one  exposure  are  filmed 
beginning  in  the  upper  left  hand  corner,  left  to 
right  and  top  to  bottom,  as  many  frames  as 
required.  The  following  diagrams  illustrate  the 
method: 


L'examplaira  film*  fut  reproduit  grAce  A  la 
giAnArositA  da: 

Library  Division 

Provincial  Archives  of  British  Columbia 

Las  imagas  suivantas  ont  At*  raproduitas  avac  la 
plus  grand  soin,  compta  tenu  de  la  condition  at 
da  la  nattet*  da  I'exemplaire  film«,  et  en 
conformity  avac  las  conditions  du  contrat  de 
filmaga. 

Les  exemplaires  originaux  dont  la  couvertura  en 
papier  est  imprim6e  sont  film6s  en  commenpant 
par  la  premier  plat  et  an  tarminant  soit  par  la 
dernlAra  paga  qui  comporta  una  empreinte 
d'impression  ou  d'iliustration.  soit  par  la  second 
plat,  salon  la  cas.  Tous  les  autres  exemplaires 
origiriaux  sont  filmAs  an  commandant  par  la 
premiere  paga  qui  comporta  una  empreinte 
d'impression  ou  d'iliustration  at  en  terminant  par 
la  dernidre  paja  qui  comporta  una  telle 
empreinte. 

Un  des  symboles  suivants  apparaitra  sur  la 
darnidre  image  de  cheque  microfiche,  selon  le 
cas:  le  symbole  — »>  signifie  "A  SUIVRE  ",  le 
symbols  V  signifie  "FIN". 

Les  cartes,  planches,  tableaux,  etc.,  peuvent  6tre 
film^s  A  des  taux  de  rMuction  diff^rents. 
Lorsque  le  document  est  trop  grand  pour  dtre 
reproduit  en  un  seul  c!ich«.  il  est  film*  A  partir 
de  I'angle  supdrieur  gauche,  de  gauche  A  droite, 
et  de  haut  en  bas,  en  prenant  le  nombre 
d'imagas  ndcessaira.  Les  diagrammes  suivants 
illustrant  la  methods. 


1 

2 

3 

1 


HflTTIE  BROWH  GObD 
MINING  COMP'Y 


Trail  Creek  Division^ 

West  Kootenay  Mining  District^ 

British  Columbia. 


OFFICERS 


J.  W.  BINKLEY, 
A.  D.  MCLAREN, 
M.   ISBISTER,  - 
WM.  AITCHISON, 


President. 

Vice-President. 

Treasurer. 

-     -  Secretary. 


TRUSTEES: 
J    W.   BiNKLEY,  A.   D,   McLaren, 

M.  ISBISTER,  WM.  AiTCHISON,  G.    C.    MOUAT. 


OFFICE  : 
Spokane,  Washington,  U.   S.  A. 


•Ht  bHf*-eO»Dtrt  CO.    dPOKAMfc. 


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HflTTIE  Bt^OWH  GOIiD 
IWINING  COIVIP'Y 


Traa  Creek  Division^ 

West  Kootenay  Milling  District, 

British  Columbia. 


OFFICERS 


J.  W.  BINKLEY, 
A.  D.  MoLAREN, 
M.   ISBISTER,  -     . 
WM.  AITCHISON, 


•    -     -     President. 

-  Vice-President. 
-     -      Treasurer. 

-  -    -  Secretary. 


M.  ISBISTER. 


TRUSTEES : 
J.  W.  BiNKLEY,  A.  D.  McLaren, 

Wm.  Aitchison,  g.  C.  Mouat. 


OFFICE  : 
Spokane,  Washington,  U.  S.  A. 


«ttJ^ 


•?S 


1+ 


Description  of  Property  and 
Expert's  Report 


OF  THE 


Jiattie  Brou/f}  (Jold  /nipii)^  Qom'y. 

CafttaIv,  1,000.000  Shares, 
Par  Value,  $  I  00  per  Share;  Fully  Paid,  Non-Asiessable. 


25o,cx)o  shares  have  been  placed  in  the  treasury 
to  be  sold  for  development  purposes. 

SPOKANE,  WASHINGTON,  U.  S.  A. 
1807. 


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Organization  and  Location. 

The  ^'Hattie  Brown  Gold  Mining 
Company"  of  Spokane,  Washington, 
is  incorporated  under  the  laws  of  the 
State  of  Washington,  for  the  develop- 
ment of  mineral  claims,  etc  ,  in  the 
United  States  of  America,  and  Province 
of  British  Columbia,  and  has  been  reg- 
istered with  the  Registrar  of  Joint  Stock 
Companies  at  Victoria,  B.  C,  and  is 


210106 


legally  qualified  to  do  business  in  that 
Province. 

This  Company  owns  the  **Hattie 
Brown''  mineral  claim,  which  is  situ- 
ated on  the  southeast  slope  of  Deer 
Park  Mountain,  in  the  south  belt  and 
about  one  (i)  mile  from  Rossland,  as 
is  shown  by  map  on  page — . 

Title. 

This  Company  has  a  perfect  title  to 
its  property,  under  Crown  Grant  is- 
sued in  March,  1896,  and  is  entirely 
free  from  debt 

Facilities  for  Mining 
and  Transportation. 

The  property  is  well  situated  on  the 
foothills  of  Deer  Park  Mountain,  fac- 
ing the  south  and  east,  and  the  prob- 
ability of  being  troubled  with  water  in 
sinking  is  very  slight;  in  fact  it  has 
been  said  there  is  almost  no  danger  to 
be  anticipated  from  this  source.  It  is 
only  about  1,000  feet  to  the  Columbia 
&  Western  Railway,  on  a  down  grade, 


and  the  cost  of  shipping  is  therefore 
reduced  to  a  minimum. 

The  Columbia  &  Red  Mountain  Rail- 
road, an  extension  of  the  Spokane 
Falls  &  Northern  Railway,  has  also 
been  built  during  the  past  season  into 
Rossland,  and  the  distance  to  the  depot 
of  this  railway  line  is  not  more  than 
one  mile. 

Assays  taken  from  various  places  on 
the  surface  run  from  a  trace  to  $125 
per  ton  in  gold,  silver  and  copper,  but 
the    highest   assays   have   only   been 
found  in  small  stringers;  however,  the 
development  work  on  the  property  up 
to  date  has  demonstrated  the  fact  that 
with  depth  the  ore  increases  in  value, 
and  from  the  enormous  showings  on 
the  property,  it  is  the  opinion  of  many 
that  a  good  body  of  pay  ore  will  be  en- 
countered before  very  great  depth  is 
attained.       Other    properties   in   this 
vicinity  have  obtained  similar  assays 
at  or  near  the  surface,  but  at  a  depth 
of  from  50  to  100  feet  have  abundance 
of  ore  that  runs  from  $25  to  $50  per 
ton  and  upwards. 


Treasury  Stock. 

This  Company  has  set  aside  250,000 
shares  of  its  capital  stock  for  the  pur- 
pose of  developing  the  property .  It 
is  being  judiciously  expended,  and  no 
officer  ot  the  Company  receives  any  re- 
muneration for  his  services;  therefore 
investors  may  feel  assured  that  they 
are  receiving  fair  treatment  from  the 
Company. 

Development  Work. 

Before  the  incorporation  of  the  '  'Hat- 
tie  Brown  Gold  Mining  Company," 
the  owners  did  considerable  exploration 
work— sufficient  to  satisfy  them  that 
in  the  ''Hattie  Brown"  they  had  a 
valuable  property.  The  work  done 
since  incorporation  will  be  found  by  ref- 
erence to  the  report  of  E.  W.  Liljegran, 
a  well  and  favorably  known  mining  ex- 
pert, who  has  resided  in  this  district  for 
several  years  and  has  been  connected 
as  superintendent  with  theLeRoi  and 
other  well-known  mines  in  the  camp. 
The  following  extracts  from  the  **Ross- 
land  Miner"  will  give  an  idea  of  the  opinion 


*r» 


V 


held  by  disinterested  parties  in  Rossland  rel-' 
ative  to  this  and  also  surrounding  properties: 

HATTIE  BROWN  IMPROVING, 

Surface  prospecting  on  the  Hattie  Brown  was  fin- 
ished before  the  recent  snowstorm  and  the  work  re;>u  ♦^ed 
in  disclosing  the  presence  of  five  veins  running  throngh 
the  property,  aU  of  which  justify  developnlen^  The 
discovery  vein  has  been  stripped  for  200  feet  Aiom  the 
old  workings  ..  » i  look?  very  strong  and  continuous. 
Work  has  ^or  the  time  being  been  concentrated  on  a 
permanent  working  shaft  which  is  being  put  down  on 
the  big  north  vein.  This  shaft  is  now  down  20  feet  and 
was  started  on  well  mineralized  vein  matter  which  is 
gradually  giving  place  to  a  solid  pyrrhotite.  A  shaft 
house  and  blacksmith  shop  are  now  being  erected. 

There  is  a  district  in  the  South  Belt  which  is  probably 
destined  to  make  a  sensation  within  the  next  few  weeks 
for  very  high  grade  ore  and  plenty  of  it.  It  is  impossible 
as  yet  to  give  the  exact  limitations  of  this  district  or  to 
describe  it  accurately,  but  it  may  be  said  to  include  the 
Silver  Bell,  Lily  May,  Curlew,  Blue  Bird,  Hattie  Brown, 
Red  Eagle,  Mayflower/  and  probably  the  Hill  Top, 
Little  Bess,  Alfe,  and  other  claims  in  that  vicinity.  The 
assays  recently  had  from  the  Mayflower,  Red  Eagle  and 
Silver  Bell  are  quite  surprising  and  leave  no  doubt  of 
the  richness  of  the  ore  in  those  claims.  A  peculiarity  is 
that  the  chief  element  of  value  in  these  ores  is  silver. 
They  also  carry  some  lead.  All  of  them  carry  gold  *  * 
*  Active  work  is  now  being  done  on  the  Silver  Bell,  Lily 
May,  Mayflower,  Blue  Bird  and  Hattie  Brown,  and  work 
is  to  commence  immediately  on  the  Red  Eagle.  We 
may  reasonably  expect,  therefore,  to  have  important  news 

from  this  gold-silver  district  at  any  time. 

7 


1 


Official  Report 

ON  THE  J*         J» 

''Hattie  Brown" 

Mineral  Qaim* 


The  *'Hattie  Brown' »  mineral  claim  is  sit- 
uated on  the  southeast  base  of  Deer  Park 
mountain,  and  is  bounded  on  the  south  by 
the  **Curlew,'»  on  the  west  by  the  ^'Lady 
DufFerin,''  on  the  north  by  the  **  Monday, V\ 
and  on  the  east  by  the  ''Blue  Bird." 

The  *'  Hattie  Brown"  has  six  distinct  min- 
eral veins  crossing  the  property,  all  of  which 
have  had  some  work  done  on  them  in  the 
way  of  partially  exposing  the  width  and 
character  of  ore. 


Mineral  Vein  No. 


I 


Vein  No.  i  is  developed  by  a  prospect 
shaft  (No.  i)  9  feet  deep,  showing  9 
feet  of  ore  and  ledge  matter.  There  is 
considerable  ore  in  which  pyrrhotite 


of  iron  predominates,  with  a  free 
sprinkling  of  arsenical  iron,  and  in 
places  quite  massive  ;  the  full  width 
of  the  vein  is  not  exposed . 

One  hundred  and  fifty  feet  north  of 
shaft  No.  I  the  vein  is  again  partially 
exposed  by  a  trench  showing  the  vein 
to  continue  well  mineralized.  The 
glacial  drift  has  left  a  .slight  covering 
of  soil  and  gravel  throughout  this  re- 
gion, which  has  covered  a  portion  of 
this  vein,  but  which,  however,  crops 
out  as  indicated  by  iron  capping. 

Mineral  Vein  No,  2. 

Vein  No.  2  has  been  developed  by  a 
shaft  and  trench  ;  the  shaft  is  13  feet 
deep,  showing  the  vein  9  feet  wide  at 
least,  the  foot  wall  not  exposed;  this 
vein  is  filled  with  porphyritic  quartz, 
containing  arsenopyrite,  iron  pyrites, 
and  iron  pyrrhotite. 

Mineral  Vein  No.  3. 

This  vein  is  developed  by  a  shaft  and 
two  open  cuts ;  the  shaft  is  down  i8 

feet,  showing  lyi  feet  of  porphyritic 

10 


\ 


1 


^ 


quartz,  with  massive  iron  pyrite  and 
arsenical  iron.  The  vein  matter  is 
quite  soft  and  the  width  has  not  been 
determined  ;  the  open  cut  on  the  east 
shows  the  well-mineralized  quartz  to 
be  at  least  5  feet  wide.  The  open  cut 
on  the  west  is  down  18  feet  in  a  soft 
oxidized  iron  vein,  well  filled  with 
kidneys  of  iron  ore,  containing  some 
copper. 

Mineral  Vein  No.  4. 

This  vein  is  devel  ^ped  by  two  shafts, 
I  open  cut  and  2  trenc  cs.  Shaft  No.  6 
is  down  13  feet  in  a  heavy  iron-capped 
vein ;  this  shows  the  whole  mass 
to  be  heavily  charged  with  iron  py- 
rites and  iron  pyrrhotite,  with  some 
copper  and  Molybdenite.  The  work- 
ings show  this  ore  body  to  be  at  least 
9  feet  wide  without  either  wall  in 
sight.  The  trenches  east  and  west 
both  show  the  vein.  Shaft  No.  5  is 
down  50  feet  in  an  enormous  iron  cap- 
ping, with  an  abundance  of  iron  pyr- 
rhotite, with  some  iron  pyrites.  The 
rock  h   :  softened  with  depth.     This 


11 


PI0106 


shaft  is  covered  by  a  shaft-house,  in 
which  is  a  blacksmith  shop  and  wind- 
lass. This  shaft  is  being  sunk  5  ft.  x  7 
ft.  in  the  clear.  It  is  intended  for  a 
general  working  shaft. 

The  vein  is   again   opened   on    the- 
east  by  an  open  cut  showing  the  lead 
to  be  very  wide  and  well-filled  with 
mineral. 

Mineral  Vein  No.  5. 

This  vein  is  developed  by  prospect 
shaft  No.  4,  7  feet  deep,  showing  the 
same  character  of  ore  as  in  vein  No.  4. 
The  width  is  not  known.     The  trench 
on  the  west  has  the  vein  continuing 
through  it;  as  it  continues  west  it  is 
covered     by    a    glacial     drift.      The 
trenches  on  the  east  show  the  con  tin - 
ation  of  the  vein    with    two   feet    of 
nearly  clean  ore,  which  is  full  of  mas- 
sive arsenical  iron,  pyrrhotite  01  iron 
and  copper.     Still  further  east  the  vein 
is  opened  by  an  open  cut  in  the  mas- 
sive iron  capping,  full    of  pyrrhotite 
ore.     The  trenches  on  the  east  show 
the  continuation  of  the  vein. 

12' 


« 


( 


Mineral  Vein  No.  6. 

This  vein  is  exposed  by  a  prospect 
shaft  4  feet  deep,  wiih  a  massive  por- 
phyritic  quartz  full  of  iron  pyrites; 
the  foot  wall  is  visible,  which  is  a  soft 
syenitic  granite;  the  ore  is  exposed  4 
feet  toward  the  hanging  wall.  This 
vein  is  visible  on  the  surface  by  the 
mineral  capping  being  exposed  east 
from  the  shaft. 


Dip  of  Veins. 


( 


Veins  Nos.   i,   2,  4,  5  and  6  all  dip 
to  the  north. 

Veins  Nos.  2,  4  and  5  dip  at  an  an- 
gle of  70  degrees. 

Veins  i  and  6  dip  at  an  angle  of  55 
degrees. 

Vein  3  dips  at  an  angle  of  60  degrees 
to  the  south. 

The  dip  and  strike  of  these  veins  is 
the  same  as  the  general  mass  of  the 
Trail  Creek  district. 

13 


In  Comparison 
with  Other  Veins. 

Veins  Nos.  4  and  5  have  the  same 
characteristic  mineral  blend  as  the  fa- 
mous *'Deer  Pirk^'  mine,  with  a  near- 
ly identical  massive  iron  capping. 
These  veins  point  directly  toward  the 
"Deer  Park,"  which  is  situated  about 
3,000  feet  to  the  west.  Veins  Nos.  2, 
3  and  6  have  the  character  of  ore  of 
the  "Blue  Bird,"  which  adjoins  the 
"  Hattie  Brown"  on  the  east.  It  is 
supposed  by  all  those  familiar  with 
this  vicinity  that  No.  3  vein  is  the 
same  on  which  the  "Blue  Bird"  shaft 
is  being  sunk,  and  this  vein  continues 
on  through  the  "Mayflower"  on  the  east. 

Formation. 

The    formation     on     the    "  Hattie 

Brown"  is  the  same  as  in  the  whole 

Trail  Creek  region,  which  is  a  diorite 

with  gabbro  in  part.     Gabbro  is  much 

more  conducive    to   ore  thai,  diorite. 

This  may  be  thejeason  why  the  Trail 

Creek  region  yields  such  liberal  returns 
on  depth. 

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Topography  and 
Shipping   Facilities. 


4 


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The  **Hattie Brown''  is  beautifully 
situated  on  the  southeast  slope  of 
Deer  Park  Mountain,  with  complete 
drainage  to  all  parts.  As  it  lies  to  the 
south  and  southeast  sun,  it  is  one  of 
the  first  to  have  bare  ground  when  the 
snow  goes  off.  In  fact,  it  is  lower 
than  the  town  of  Rossland,  and  within 
twenty  minutes'  walk  of  town.  There 
is  a  good  wagon  road  as  well  as  a  rail- 
road to  the  property — the  wagon  road 
crossing  the  southwest  corner  and  the 
railroad  passes  within  i,ooofeet  to  the 
east,  affording  excellent  shipping  facil- 
ities, being  an  all  down  grade  from 
the  mine  to  the  railroad  track. 


Remarks. 


The  **riattie  Brown"  enjoys  many 
superior  features  and  advantages  over 
the  majority  of  mineral  claims. 
Firstly,  the  great  number  of  min- 
eral veins  crossing  the    property,  the 


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widths  of  which  are  not  known. 
Secondly,  its  nearness  to  town,  that 
it  can  be  reached  and  worked  to  ad- 
vantage the  whole  year.  Thirdly, 
its  excellent  transportation  facilities. 
Fourthly,  with  a  stream  of  water 
crossing  the  southwest  corner,  afford- 
ing an  abundance  for  all  purposes. 


Opinion. 


It  is  my  opinion  that  within  the 
lines  of  the  *' Hattie  Brown"  depth 
will  yield  in  several  places  vast  quan- 
tities of  valuable  ore. 

Respectfully  yours, 

E.  W.   LlLJEGRAN,  M.  E. 

Investigation  Asked. 

Intending  investors  are  invited  to 
make  the  closest  inquiry  as  to  this 
property  as  well  as  to  the  standing  and 
character  of  the  directorate.  This  is 
put  forth  as  a  thoroughly  legitimate 
mining  venture  and  the  most  scrupu- 
lous regard  will  be  had  for  the  interest 
of  every  subscriber. 

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